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Table 2

List of H2O transitionsa detected with PACS in L1157–B1, at the nominal position of B1 (spaxel centered at offset (0′′,0′′)) and at the high-J CO peak (spaxel at offset (−5′′,7′′)).

Transition Frequency λ Eu/kB HPBW Fluxb Line_Id

(GHz) (μm) (K) (arcsec) (× 10-17 W m-2/pixel)
offset (0′′,0′′) offset (−5′′,7′′)

o-H2O 221 − 212 1661.008 180.49 159.8 12.7 2.6 ± 0.2 2.7 ± 0.3 1
 212 − 101 1669.905 179.52 80.1 12.7 12.1± 0.2 12.9 ± 0.3 2
 303 − 212 1716.769 174.63 162.5 12.3 6.2± 0.3 6.5 ± 0.3 3
 423 − 414 2264.149 132.41 397.9 9.4 <0.6c 0.6 ± 0.2 4
 414 − 303d 2640.474 113.54 289.2 8.0 2.8 ± 0.5 3.7± 0.4 5
 221 − 110 2773.978 108.07 159.8 7.6 3.2 ± 0.4 3.9 ± 0.5 6
 321 − 212 3977.046 75.38 271.0 5.3 <2.1c 1.9 ± 0.7 7
p-H2O 313 − 202 2164.132 138.53 204.7 9.8 2.7 ± 0.3 2.7 ± 0.3 8
 404 − 313 2391.573 125.35 319.5 8.9 1.1 ± 0.3 1.4 ± 0.3 9

Notes.

(a)

Frequencies taken from the JPL spectroscopic catalog (Pickett et al. 1998).

(b)

Line fluxes obtained with a Gaussian fit of the line profile.

(c)

3σ upper limit based on the rms estimated at offset (− 5′′,7′′).

(d)

This line is blended with the CO (23–22) transition. To estimate the flux of the water line we subtracted the flux of CO (23–22) transition predicted by the model presented in Benedettini et al. (2012).

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